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Characteristics of magnetic fabrics of Jiangshan-Shaoxing collision belt and its tectonic implications

机译:江绍绍碰撞带磁性织物的特征及其构造意义

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摘要

The study of anisotropy of magnetic susceptibility(AMS)of rocks from the northern part of Jiangshan-Shaoxing collisional belt demonstrates that the minimum principle AMS axes are the most concentrated one in various types of rocks. The planar projection of the minimum axis shows that the main compressive stress lies on northwest 30°-60°, which trends domi- nantly in northwest-southeast of Chencail area and arc-like disperse towards both north and south of Chencail.
机译:对江山—绍兴碰撞带北部岩石磁化率(AMS)各向异性的研究表明,最小AMS主轴是各类岩石中最集中的。最小轴的平面投影表明,主压应力位于西北30°-60°,在Chencail地区的西北东南部占主要趋势,并且向Chencail的北部和南部呈弧状分散。

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